Changes between Version 18 and Version 19 of 2020WP/TOP-01_rlod_Antarctic_ice_Sheet_Fe_Source

Timestamp:

2020-11-27T15:15:45+01:00 (3 years ago)

Author:

rlod

Comment:

--

2020WP/TOP-01_rlod_Antarctic_ice_Sheet_Fe_Source

@@ -23 +23 @@
 
 
-Based on the development done with NEMO 3.6 of the representation of the missing external source of Fe from iceberg and ice shelf in the PISCES model
+Based on the development done with NEMO 3.6 of the representation of the external source of Fe from iceberg and ice shelf missing in the PISCES model.
 
 
@@ -29 +29 @@
 
 Representation of the external source of biogeochemical tracers from iceberg and ice shelf.
-For instance, for dissoved Fe, a sediment content associated to a solubility fraction of sediment Fe is added to the freshwater fluxes of iceberg and ice shelf. For iceberg, a homogeneous distribution of the biogeochemical tracers until 120 m of depth is applied. For ice shelf, the biogeochemical tracer content is distributed homogeneously following the representation of the isf freshwater flux of Mathiot et al. (2017) whether the under ice shelf cavities are open or not. 
+For instance, for dissoved Fe, a sediment content associated to a solubility fraction of sediment Fe is added to the freshwater fluxes of iceberg and ice shelf. For icebergs, a homogeneous distribution of biogeochemical tracers is applied from the surface to a depth that can be selected in the namelist_top. For the time being, a distribution down to a depth of 120 m is recommended. For ice shelf, the biogeochemical tracer content is distributed homogeneously following the representation of the isf freshwater flux of Mathiot et al. (2017) whether the under ice shelf cavities are open or not. 
 
 File dependency: feshwater fluxes from ice shelf and iceberg: